MOE Key Lab of Marine Reservoir Evolution and Hydrocarbon Enrichment Mechanism, China University of
Geosciences (Beiing) MOLR Key Lab of Shale Gas Resources Survey and Strategic Evaluation, China University
of Geosciences (Beijing) China United Coalbed Methane Corporation Ltd.

为研究沁水盆地南部柿庄南煤层气开发区块山西组3号主采煤层的地下水径流与水化学特征,从该区采集了煤层气井排出水样,对主要离子浓度进行测定,并分析离子浓度展布特征。研究结果表明:研究区水质类型以Na-HCO3-Cl或Na-HCO3型为主;由东向西呈现出水文径流区（氧化环境）到滞流区（还原环境）的过渡特征,受控于矿物溶解反应,KDS、Na+、K+、Cl-、Ca2+、Mg2+、HCO3-等离子浓度由东向西逐渐增加,SO42-由于脱硫酸效应呈相反变化趋势,高产井多分布于高矿化度、高离子浓度的区域,离子浓度与矿化度指示了研究区的地下水径流特征,可以作为判断煤储层水动力条件与开发有利区的参考因素。

In order to study the groundwater runoff and water chemistry characteristics of the No. 3 Shanxi Formation coal reservoir in Shizhuangnan Block, Southe rn Qinshui Basin, the authors collected water samples from coalbed methane wells. The characteristics of ion concentration were determined to analyze the distribution characteristics of ion concentration. The results showed that the water types of the water samples in study area were mainly Na*-HCO3-CI and Na*-HCO3- type; the st udy area had the characteristics of the transition from the runoff area ( oxidation environment) to the residence area ( reduction environment) from east to west. The co ncentration of KDS, Na+, K+, CI, Ca2+, Mg2+ and HCO3~ which increased gradually from east to west were controlled by mineral dissolution reaction, while under the d e sulfate effect, the concentration of sO42- was gradually decreased. High production wells were mainly distributed in high salinity and high ion concentration region. K DS and ion concentration indicated the characteristics of groundwater flow in the study area and can be used as reference factors for judging the runoff conditions of co al seam water and evaluating exploration target.

国家科技重大专项资助项目(2011ZX05060,2011ZX05034-003)；国家科技支撑计划资助项目(2014BAC18B02)；